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Scientific Drilling
Scientific Drilling

... Topics needing special attention include the influence of subseafloor microbes on Earth and ocean history, the influence of subseafloor microbes on local and global cycling of carbon, nitrogen, phosphorus, sulfur and a host of other elements. More specific topics include (i) the role of microbes in ...
Phosphorus cycling in the Sargasso Sea: Investigation
Phosphorus cycling in the Sargasso Sea: Investigation

... North Atlantic. They concluded this activity was due to enhanced utilization of the DOP pool in response to high levels of nitrogen fixation, forcing the system towards P-limitation. The third line of evidence is rapid turnover times above the thermocline (4 - 8 hours) that increases with depth to ...
Chapter 4 _5_
Chapter 4 _5_

... Aquatic habitats are warmer near the equator and colder near the poles. Temperature in aquatic habitats also often varies with depth. The deepest parts of lakes and oceans are often colder than surface waters. Currents in lakes and oceans can dramatically affect water temperature because they can ca ...
Using Space-Age Technologies to Monitor the Coast`s Health
Using Space-Age Technologies to Monitor the Coast`s Health

... A satellite detects visible and infrared light reflected from features on land, from farmland to construction areas. The amount of light reflected varies by feature or, in the case of a marsh, by plant type. Each marsh plant species has a unique “spectral signature,” and Klemas and his team have lea ...
Plate Tectonics Webquest
Plate Tectonics Webquest

... Roll your mouse over the image to find the definitions of the words below: Subduction Zone - Area where one plate is being pulled under another. Magma – Molten rock, gases, and solid crystals and minerals. Trench – A steep sided depression in the ocean floor. Volcano – A vent in the earths surface t ...
Key Concept Review (Answers to in-text “Concept Checks”) Chapter
Key Concept Review (Answers to in-text “Concept Checks”) Chapter

... 13. The bulk of neritic sediments are terrigenous; they are eroded from the land and carried to streams, where they are transported to the ocean. 14. Neritic sediments can undergo lithification: They are converted into sedimentary rock by pressure-induced compaction or by cementation. 15. Much of th ...
scientific synthesis on the impacts of ocean fertilization on
scientific synthesis on the impacts of ocean fertilization on

... activities; with the exception of small scale scientific research studies within coastal waters. Such studies should only be authorized if justified by the need to gather specific scientific data, and should also be subject to a thorough prior assessment of the potential impacts of the research stud ...
Geology of Paraná
Geology of Paraná

... on the coastal plain. There, and all over Serra do Mar and the First Paraná Plateau, igneous and metamorphic rocks of Archean to early Paleozoic age outcrop in the region known as the PARANÁ SHIELD, whose strong relief reflects how resistant to weathering its rocks are. ...
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Bathymetric stripping corrections to gravity gradient components Robert Tenzer and Pavel Nov´ak

... apparatus of the spherical harmonic analysis and synthesis. Novák (2010) computed globally the gravitational potential generated by the global ocean masses with a very high spatial resolution. In these studies a constant value of the ocean density contrast was adopted. The actual seawater density v ...
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Plate Tectonics

... EQ: How is Earth’s crust changed by plate movements? Plate Tectonics: Welcome to the greatest show on Earth. Propelled by intense heat simmering beneath the crust or the mantle, Earth’s surface is dramatically reshaping itself in an endless, slow-motion movement called plate tectonics. Tectonic plat ...
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1 Central Arctic Ocean paleoceanography from ~50 ka to present, 1

... Krithe typically signifies cold well-ventilated deep water and perhaps low food supply (Poirier et al., 2012 and references therein). Krithe is also a dominant component (>30%) of North Atlantic Deep Water (NADW) in the subpolar North Atlantic Ocean. Its abundance varies during glacial-interglacial ...
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Prediction of Tele-Tsunami from Canary Island on the West African

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GEO/OC 103 Exploring the Deep… Lab 7

... water available in the oceans. Carbon dioxide is also abundant in ocean waters. It is released as a by-product of respiration, and it is readily absorbed into the ocean from the atmosphere. Thus, water and carbon dioxide are not limiting resources for photosynthesis or primary productivity in the oc ...
"Dynamic Earth Guided Notes" (Plate Tectonics)
"Dynamic Earth Guided Notes" (Plate Tectonics)

... ~ Example: Himalayas, Appalachians, Alps (mountains) ~ Regional Metamorphism: Formation of metamorphic rock bodies that are hundreds of square kilometers in size. ...
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The Cherry - The Woodlands of Ocean Pines

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Sea Floor Spreading and Plate Tectonics
Sea Floor Spreading and Plate Tectonics

...  Until the mid-1900s, most people, including ...
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... There is a third group of complex waves, collectively known as L waves. They are made up of waves which move in elliptical or horizontal transverse motions. They are generated at the surface when P and S waves reach there. L waves travel only on the surface of the Earth and are responsible for most ...
Chapter 18
Chapter 18

... the upper part of the mantle. It is made up of rock. It is the “strong layer”. The lithosphere is comparatively rigid plates that are moving, floating in the upper mantle like giant ice sheets floating in the ocean. The continental drift. Earthquakes, volcanoes, and most rapid changes in the earth’s ...
The Sea Floor
The Sea Floor

... terrigenous: derived from land and brought to sea floor …sands/silts that make up continental rise… pelagic: accumulate by settling through water column …clays from wind; skeletons of microsopic organisms… ...
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AOOS - Summer 2015 Newsletter

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Cross Section: Plate Tectonics - Oologah

... divergent boundaries, are where plates of the Earth’s crust move away from one another. Convergence, or convergent boundaries, are where plates of the Earth’s crust move towards one another. You can see examples of two kinds of boundaries in your lab manual on page 42, Figure 2.10. Plates – The crus ...
Investigation of Seasonal Variation of Wave Energy Density around
Investigation of Seasonal Variation of Wave Energy Density around

... wave power generation at Jeju sea which is considered to contain the highest wave energy density in Korean coastal waters. The spatial and seasonal variation of wave power per unit length is calculated in Jeju sea area based on monthly mean wave data from 1979 to 2002 which was produced by SWAN wave ...
Answer the following: Answer the following: Draw a
Answer the following: Answer the following: Draw a

... rocks on each side of a fault are moving slowly. If the fault is locked, stress in the rock increases. When a rock is stressed past a certain point, the rocks fracture, separate at their weakest point, and then spring back to their original position. ...
Short Bibliography on current European Marine Biotechnology
Short Bibliography on current European Marine Biotechnology

... cosmetics, artificial bone, biosensors, bioremediation, foods, biofuels, etc. The Atlantic Ocean is the second largest ocean on earth, extending to the poles and including the sub-tropics – its biodiversity is high encompassing a huge range of habitats. Rationale Identification of relevant European ...
Aluminium in an ocean general circulation model compared with the
Aluminium in an ocean general circulation model compared with the

... with a nominal resolution of 2◦ × 2◦ , with the meridional resolution increased near the equator and two ‘north poles’ in Canada and Russia to eliminate the coordinate singularity in the Arctic Ocean. Its vertical resolution is 10 m in the upper 100 m, increasing downward such that there are 30 laye ...
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Physical oceanography



Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.
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